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an engineering geological characterisation of tropical clays - GBV

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1<br />

Chapter 1<br />

Introduction<br />

1.1 Scope <strong>of</strong> study<br />

The purpose <strong>of</strong> this project was to study <strong>an</strong>d evaluate <strong>engineering</strong> <strong>geological</strong> characteristics <strong>of</strong> soils<br />

found in the Nairobi area, Kenya. The information <strong>an</strong>d data so obtained would be useful for<br />

assessing the suitability <strong>an</strong>d capacity <strong>of</strong> soils found regarding the possibilities <strong>an</strong>d / or limitations <strong>of</strong><br />

developing <strong>an</strong>d constructing low buildings <strong>an</strong>d other light <strong>engineering</strong> structures ( roads, pavements<br />

etc) in the study area <strong>an</strong>d <strong>geological</strong>ly similar neighbourhoods. Attempts have been made by the<br />

author to present the <strong>geological</strong> data <strong>an</strong>d soil parameters in a spatial continuous form that would be<br />

readily useful <strong>an</strong>d applicable by <strong>engineering</strong> geologists, geo-engineers <strong>an</strong>d pl<strong>an</strong>ners <strong>of</strong> futureintended<br />

construction projects in the area. The results <strong>of</strong> the investigations together with related<br />

<strong>engineering</strong> <strong>geological</strong> assessments would assist especially at the stages <strong>of</strong> pl<strong>an</strong>ning, designing <strong>an</strong>d<br />

construction <strong>of</strong> projected facilities; <strong>an</strong>d also subsequent mainten<strong>an</strong>ce after completion.<br />

The current study area lies mainly to the south <strong>of</strong> the fast growing Nairobi city, Kenya. However,<br />

the southern half <strong>of</strong> the Nairobi metropolit<strong>an</strong>, including the City centre, is also covered. The area is<br />

covered by topographic sheet 148/4 <strong>of</strong> Nairobi, at a scale <strong>of</strong> 1:50 000; <strong>an</strong>d printed by the Survey <strong>of</strong><br />

Kenya (1991). The exact location <strong>an</strong>d extent <strong>of</strong> the study area is described in the next section. The<br />

area is covered mainly by varying thickness <strong>of</strong> black cotton soils. Occurrences <strong>of</strong> red soils are also<br />

found, but limited in the north-western part <strong>of</strong> the area. Underlying the soils are Tertiary volc<strong>an</strong>ics<br />

which in turn overly a Basement system <strong>of</strong> folded Precambri<strong>an</strong> metamorphic rocks.<br />

The present area was chosen because it is mainly located on the outskirts <strong>of</strong> Nairobi city which are<br />

projected for future exp<strong>an</strong>sion <strong>of</strong> the town, as regards construction <strong>of</strong> new social-economic <strong>an</strong>d<br />

industrial facilities, residential houses <strong>an</strong>d related infrastructure. It is also largely covered by the<br />

potentially exp<strong>an</strong>sive <strong>an</strong>d reactive, relatively unstable <strong>an</strong>d problematic black cotton soils. Previous<br />

works <strong>an</strong>d studies in adjacent areas <strong>an</strong>d sections <strong>of</strong> the present area (Anyumba, 1991; M<strong>an</strong>ga,<br />

1988; Mowlem, 1985), together with recent field observations by the author reveal problems <strong>of</strong><br />

ground instabilities, failures <strong>an</strong>d movements in areas <strong>of</strong> black cotton soils with serious <strong>engineering</strong>,<br />

environmental <strong>an</strong>d social-economic implications.<br />

The field study phase <strong>of</strong> this project was carried out in Nairobi (Kenya) in the period <strong>of</strong> April-<br />

September, 1999; <strong>an</strong>d December, 2000-J<strong>an</strong>uary, 2001. The laboratory study phase was undertaken<br />

in the period <strong>of</strong> November, 1999-March, 2001; based at the Department <strong>of</strong> Engineering Geology,<br />

Institute <strong>of</strong> Geology <strong>an</strong>d Palaeontology, Technical University <strong>of</strong> Clausthal-Germ<strong>an</strong>y. The field<br />

methods <strong>an</strong>d laboratory procedures followed in the investigation, study <strong>an</strong>d <strong>an</strong>alysis <strong>of</strong> the soils <strong>an</strong>d<br />

underlying bedrock are summarised in the relev<strong>an</strong>t sections in later chapters.<br />

Adequate <strong>an</strong>d proper <strong>engineering</strong> <strong>geological</strong> studies <strong>an</strong>d investigations should serve to provide<br />

useful <strong>an</strong>d detailed information on aspects <strong>of</strong> geology (rock types <strong>an</strong>d lithostratigraphy), types <strong>of</strong><br />

soil, geomorphology <strong>an</strong>d <strong>geological</strong> structures, hydrology <strong>an</strong>d hydrogeology, <strong>an</strong>d geotechnical<br />

characteristics <strong>an</strong>d potential behaviour <strong>of</strong> rocks <strong>an</strong>d/ or soils; followed by <strong>an</strong> assessment <strong>of</strong> potential<br />

instabilities <strong>an</strong>d possible natural hazards, <strong>an</strong>d a subsequent consideration <strong>of</strong> suitable development<br />

projects (Attewell, 1976; Bell <strong>an</strong>d Pettinga, 1985; Blyth, 1974; Hedberg 1976; Sowers, 1994;<br />

Tilford, 1994). In addition to the above investigations, this study also includes a detailed chemical<br />

<strong>an</strong>d mineralogical <strong>an</strong>alysis <strong>an</strong>d evaluation <strong>of</strong> the soils <strong>of</strong> the area. Genetic aspects <strong>of</strong> the soils are<br />

also discussed.

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